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国家地下水监测工程数据在地下水动态月报评价中的应用效果浅析 被引量:9

Application of National Groundwater Monitoring Project Data in Monthly Report of Groundwater Dynamics
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摘要 地下水动态月报是水利部门定期发布地下水情的重要平台之一,传统的地下水监测数据收集方法使得月报发布存在滞后明显的现象。国家地下水监测工程(水利部分)的建设为月报编制工作提供了更加及时、覆盖面更广的监测网络和数据信息。选取江苏北部平原区与辽宁中部平原区为代表,对比分析了国家地下水监测工程监测数据与传统人工上报地下水数据,定量描述了两类数据表达区域地下水埋深空间分布特征的差异。研究表明,国家地下水监测工程的地下水监测站点分布和数量要优于历史人工测站的分布情况。 The monthly report of groundwater dynamics is an important production showing the groundwater regimen in the main plains of the North China released by Ministry of Water Resources.The traditional method of manual collecting made serious delay of the monthly report publication.Parts of the national groundwater monitoring project,constructed by Ministry of Water Resources,provide a more extensively monitoring network and timely groundwater monitoring data.In this paper,the northern plain of Jiangsu and the central plain of Liaoning were selected as two cases.The two kinds of data sources of the monitoring data collected from the national groundwater monitoring project and the traditional method were comprehensively analyzed,and the differences in the spatial distribution of the groundwater depth were quantitatively described.This research shows that the spatial distribution and quantity of the groundwater monitoring stations in the national groundwater monitoring project are better than those derived from the manual stations.
作者 杨桂莲 宋凡 鲁程鹏 吴昊晨 赵庆鲁 YANG Guilian;SONG Fan;LU Chengpeng;WU Haocheng;ZHAO Qinglu(Information Center,Ministry of Water Resources,Beijing 100053,China;College of Hydrology and Water Resources,HohaiUniversity,Nanjing 210098,China;Hydrology and Water Resources Center for Middle Reach of Heilongjiang River,HydrologyBureau of Songliao Water Resources Commission,Jiamusi 156499,China;Liaocheng Hydrology Bureau of Shandong Province,Liaocheng 252000,China)
出处 《水文》 CSCD 北大核心 2019年第5期45-49,24,共6页 Journal of China Hydrology
关键词 国家地下水监测工程 地下水动态月报 埋深等值面 national groundwater monitoring project groundwater dynamics monthly report groundwater depth isosurface
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